308
Chemical Oceanography, 4th Edition
0
500
1000
1500
2000
2500
3000
60°
50°
40°
Atlantic
Pacific
Indian
30°
20°
10°
0°
10°
20°
30°
40°
50°
60°
60°
50°
40°
30°
20°
10°
0°
10°
20°
30°
40°
50°
0 10 20 30
Anthropogenic
CO 2
(µmol/kg)
Saturation Levels
Present Aragonite
Pre-Industrial Aragonite
Pre-Industrial Calcite
Present Calcite
60
40 50
60°
50°
40°
30°
Latitude
20°
10°
0°
10°
20°
Pressure (db)
0
500
1000
1500
2000
2500
3000
Pressure (db)
0
500
1000
1500
2000
2500
3000
Pressure (db)
Figure 7.47
Effect of fossil fuel CO 2 on the saturation levels in the oceans. (From Feely, R.A., Sabine, C.L., Lee, K., Berelson,
W., Kleypas, J., Fabry, V.J., and Millero, F.J., Science, 305, 362, 2004. With permission.)
Chemical Oceanography, 4th Edition
0
500
1000
1500
2000
2500
3000
60°
50°
40°
Atlantic
Pacific
Indian
30°
20°
10°
0°
10°
20°
30°
40°
50°
60°
60°
50°
40°
30°
20°
10°
0°
10°
20°
30°
40°
50°
0 10 20 30
Anthropogenic
CO 2
(µmol/kg)
Saturation Levels
Present Aragonite
Pre-Industrial Aragonite
Pre-Industrial Calcite
Present Calcite
60
40 50
60°
50°
40°
30°
Latitude
20°
10°
0°
10°
20°
Pressure (db)
0
500
1000
1500
2000
2500
3000
Pressure (db)
0
500
1000
1500
2000
2500
3000
Pressure (db)
Figure 7.47
Effect of fossil fuel CO 2 on the saturation levels in the oceans. (From Feely, R.A., Sabine, C.L., Lee, K., Berelson,
W., Kleypas, J., Fabry, V.J., and Millero, F.J., Science, 305, 362, 2004. With permission.)
